Three-Dimensional Modeling of Tsunami Generation and Propagation under the Effect of Stochastic Seismic Fault Source Model in Linearized Shallow-Water Wave Theory

Figure 20

The variance of the propagated tsunami waveforms for different propagated uplift length 𝐿, 𝐷=50km, ℎ=2km, and 𝑡=300/𝑣, where 𝑡^∗=𝐿/𝑣 and 𝑣=𝑣_𝑡.

(a) For 𝐿=50 at 𝑡=6𝑡^∗

(b) For 𝐿=100 at 𝑡=3𝑡^∗

(c) For 𝐿=150 at 𝑡=2𝑡^∗

(d) Side view for 𝐿=50,100,150